-

Application o Tienin Arid Zone €$dmlo"y (Proceedings of the %en~~Symposium, Augur1 1994fIAHS Publ. no. 232. 1 95. 285

;tionally . Onthe conduc- Isotopic study of rainfall in the Sahelian zone () atistical along two sections, east-west (Lake -) and ge-scale north-south (-Niamey) ifersin ìtions of J. D. TAUPIN n wells. ORSTOM,Mission au Niger, BP 11416, Niamey, Niger milar to velocity R. GALLAIRE ons and ORSTOM,LHGI, Université Paris XI, 91400 Ceder Orsay, France ydraulic J. CH. FONTES 'y saline LHGI, Université Paris XI, 91400 ,Ceda Orsay, France iuctivity y distri- Abstract During two years (1988, 1989) a study of rainfall isotopic de up to content (2H, "O) was carried out in Niger. This study aimed at analysing 1. the average oxygen-18 and deuterium contents of rainfall at the time scale of con- of a storm at six stations in 1988 and 12 stations in 1989, spread out xion of along two sections: east-west*(LakeChad-Niamey) which is the prevai- n at the ling direction of the mesoscale convective systems (MCS)circulation and e above north-south (Agadez-Niamey). These intersections are representative of I I j lack of the different rainfall regimes of the (100-800 mm). The oxygen-18 aquifer. .y, content of rainfall varies by more than 12%0.The isotopic composition :h allow at the beginning of the season seems to be more enriched with heavy iso- ption of topes, which can be directly connected to the low rainfall amounts and the significant evaporation of water drops when falIing through the atmosphere characterizing this period. The most depleted values are reached in August, the wettest month, when the vertical development of clouds is likely to be the strongest. The isotopic content of rainfall at the i limit of the Saheliwzone is influenced by the evaporation during the -145. whole rainy season. The isotopes have also been used in order to follow ermination the isotopic composition of the MCS during their travel over Niger, so mer), 193- as to check on the one hand the hypothesis of an opposite continental 4rabia (ed. effect, and on the other the process of water vapour feeding the system. y Period in

,lirol. 112, INTRODUCTION

Qatar. In: The air mass circulation in Niger and in Sahelian Africa is mainly influenced by the anti- cy6lone of the Azores in the north, which engenders hot and dry air called "Harmattan" upon Sahara, and the anticyclone of Saint Helen to the south of the Equator, which gene- rates a fresh and wet air mass &ed the "Guinean Monsoon". The annual latitudinal oscillation of the zone of confrontation between these two flows causes the alternation of dry seasons (October-March) andhumid seasons (April-October), which is charac- teristic of the dry tropical climate. The Inter Tropical Front 0symbolizes at ground level the limit between these two air-masses. Precipitations in that region depend almost

_- .-

.'Y

286 J. D. Taupin et al. ITF solely on the position of the and on its structure, which can be distinguished by a vertical discontinuity of wind and wetness fields. Due to such a structure, 80% of rains in the Sahel have a convective origin, either in the form of isolated thunderstorms, or in the form of coherent cloudy accumulations which move from east to west at a speed that can reach 60 Ion h-' called squall lines.

METEIODOLOGY The zone studied is situated between 12" and 17"N and 1" and 14" E. The sampling (Fig. 1) has been made at six stations in 1988 (Niamey, Brini N'Konni, , Agadez, Maradi and ) in apartial way. In 1989, a systematic sampling at the scale of an event has been made from June to October in these stations and in six others (Tillabéri, Gaya, Chikal, Goure, , N'Guigmi). The isotopic analysis of oxygen-18 (6180)and deuterium (a2H) have been made that year on more than 90% of rainfalls in each station, except those of Tillab6ri and Gaya, not yet analysed. Temperatures and relative humidity have been measured before and just after each rainy event.

RESULTS

The first results of the study show that the isotopic contents range from -9.33 to +5.15 %O in the case of oxygen-18 and from -65.5 %O to +32.0 %O for deuterium. The most positive values, which show an enrichment in 6"0, are due to rain evaporation during its fall through an unsaturated atmosphere. In Fig. 2, which describes the distri- bution of isotopic contents of oxygen-18 during the rainy season at five stations, it can be noted that at the beginning of the season, values are not much negative or even posi-

Fig. 1 Location of research area. Isotopic study of rainfdl in the Sahelian zone (Nìgm) 287

150 170 190 210 230 250 270 Time (day) Fig. 2 Evolution of the oxygen-18 contents of rainfall during the 1989 rainy season.

tive. Such a phenomenon can sometimes be observed at the end of the season. At the mid-season (July and August), values are a lot more depleted in oxygen-18. That can be directly linked to the,growth and raising of the monsoon flow to the north, At the beginning of the season, the monsoon is not yet well installed, bringing conditions which do not ease rainfalls; on one hand rainfalls are weak and on the other hand the atmos- phere, generally unsaturated, is a factor of re-evaporation. This process of re- evaporation is particularly important in the most northern stations (Agadez and Tahoua) and in the most eastern ones (Diffa, Gour6 and N'Guigmi), where annual rainfalls are the weakest, because the conditions of saturation are rarely obtained during the whole rainy season. In Fig. 2, the isotopic tendency of the station at Agadez is linked to that of the other stations: enriched isotopic contenti at the beg'inning and at the end of the season and depleted isotopic contents during the mid-season, but isotopic contents are always more enriched, compared to the other stations. The same process, although less remarkable, can be noted in the case of the eastern stations. In Table 1, showing the weighted mean annual isotopic composition of precipitation for each station, a very clear enrichment to the south-northtransact (Bimi N'Konni, Tahoua, Agadez) can be noted, from -3.72%0 to -0.30% in oxygen-18. The east-west section also tends to enrich to the east, between Niamey and Diffa, from -4.54 %O to - 1.82%. But the station of "Guigrni, the most eastern one, whose annual rainfall is 109 mm, has a particularly depleted weighted meap. annual isotopic composition of precipitation (-4.54 %O in oxygen-18). That unusual content can be linked to three exceptional events, very depleted in oxygen-18, in August, bringing more than 60% of the total rainfall. Of course the weighted mean annual isotopic composition of precipitation in that station might be important; so the isotopic content cannot be considered as an average inter- annual content. Evaporation is also well linked to the average relative humidity during rainfall (Fig. 3). It can benoted that, from an oxygen-18 content of about -2%0, the decreasing of the relative humidity is linked to the isotopic enrichment. The same analysis could have been applied to the temperature, which is linearly correlated to the relative 288 J. D. Taupin et al. - 100 .A m i %soAo. .yOm .A Ad ma n +e A* ' E 80- A A 0.4 moAA4rnbA.L. .Im3 0 4. - .A o'+ o 'a + 0. 3 60- BAO Ao & A.

0.92, humidity (3 = 0.65 to depending on the station). In the case of Agadez, the atmosphere under the cloud always keeps the air far from saturation, which explains the large dispersion of values. The relation between oxygen-18 and rainfall (Fig. 4) shows the mass effect that can be observed in a tropical climate; but it can also be noted that some rainfalls are very depleted, though the rainfall depth is small. That can be linked to the mechanism of convection which, contrarily to what happens in the case of monsoon rainfalls, can have an important vertical development, to between 10 O00 and 15 O00 m high. Such heights bring very low condensation temperatures so very negative isotopic contents which do

- 120 . 1001001 - BlRNlN'KONNI 0 TAHOUA

A ZMDER GOURE 0 DIFFA * N'CUIGMI + ACADEZ A

-10 -8 -6 -4 -2 . o 2 4 6 oxygen 18 t%oVs SMOW) Fig. 4 Relationship between oxygen-18 contents and depth of rainfall. not have time to re-equilibrate with the ambient temperature during the fall of raindrops. Such convective movements are particularly abundant in July and August, where clima- i tological conditions are combined to allow the development of convection at a regional scale. In the oxygen-18 versus deuterium graph (Fig. 5, Table 1) rainfalls axe situated i 1 I1 around the Waters Meteoric Line (WML), whose equation is: S2H= 8.S1'0 + 10. For different stations, the value of the slope A of the linear relation S2H= A.S1'O + B ranges from 5.1 to 7.1 for all rainfall. If only non-evaporated rainfalls axe taken into I' consideration, the dope increases a little and ranges from 6.4 to 8.0. By taking only the stations with the most important rainfalls (Niamey, Birni N'Konni, Maradi and Zinder) where the evaporation process is less remarkable, the relation tends to that found by Joseph & Aranyossy (1989) established from the isotopic composition of the Sahelian band superficial groundwaters, which is: S2H = 7.5.S1'0 + 4.8. It can be noted that many points are substantially above the meteoric line, which concretizes by an excess of deuterium d = S2H - 8.S1'0 superior to 10, due to the non-negligible contribution of recycled continental water to rainfalls. The comparison between the years 1988 and 1989 shows the difference of the weighted mean annual isotopic composition of precipitation that can exist between a rainy season considered as normal (1988) and a season showing a deficit over the zone (1989). The consequence is, in the case of Bimi N'Konni, a weighted mean annual isotopic composition of precipitation equal to -4.41 % (546 mm) in oxygen-18 in 1988 and -3.72% (450 mm) in 1989. The annual isotopic characteristic will principally depend on the isotopic contents of August which associates the important rainfalls with the most depleted isotopic contents. That is what can be noted at Bimi N'Konni where the important rainfalls in August 1988,285 mm compared to 165 mm in 1989, will have a great annual influence (Fig. 6). Mathieu et al. (1993) tie the depletion of the isotopic composition to the maximum evolution of the monsoon further north in 1988, and to the presence of more numerous convective c$lls. Still, kcan be noted that in 1989 the

O

.+I

0 O0 ONUMEY OcHncAL BlRMN'KONNI A MARADI A ZINDER e GOURE .- n WGUIGMI e DETA 0 TAHOUA + ACADEZ O -10 -8 -6 -4 -2 2 4 6 vs 18 oxygen (%O SMOW) Fig. 5 Relationship between oxygen-18 and deuterium. J. D. Taupin et al.

Table 1 Relationshipbetween oxygen-18 (%) and deuterium eH) and weighted mean annual isotopic composition ofprecipitation for each station. -tb& r2 dcpbJt Number of A B Rainfall Annual Annual samples (mm) mean mean ’“’Y Qn 180 28 Shows Niamey 24 6.032 -4.663 0.841 599.8 -4.54 -339 e 6.751 -0.493 0.837 squall li -229 Qlilral u) 5.136 -12674 0.732 2755 -1.75 the sign 6.712 -5.172 om7 reveals Bhi N’Konni 30 6.w) 2869 0.919 449.9 -3.72 -188 6.773 5.450 0.904 and lesr Tahoua 25 6.391 -3.709 0.710 362.4 -213 -24.6 7.639 3.133 0.926 relative A* 13 5.151 0.848 0.726 130.3 -0.3 -1.76 lot gra 7.031 1.493 0.894 oceanic Maradi 26 7.194 3.010 0.852 586.7 -3.87 -226 8.078 7.301 0.887 tuted b: zinda 21 6.782 2.505 0.909 317.6 4.U -24.6 7.197 4.603 0.860 God 18 5.a40 -1.802 0.929 2893 -258 -155 6.455 0.947 0.878 Diffa 16 6.137 -0.183 0.882 m.8 -1.82 -10.1 6.520 1.292 0.921 NGuigmi 10 6.401 -6.958 0.975 108-7 4.38 -355 6.862 4.463 0.940 Niamcv. Birni. 7.281 4,982 0.870 Maradi; .Znd& isotopic contents.duringthe first two ten-day periods of August were a lot more depleted than in 1988, which can be due to high-altitude convection events that did not occur in 1988 at such an altitude. So, an important evolution of the monsoon to the north would block high-altitude convections. A study of temperature data at the top of clouds (infra- red satellite ìmages) would permit one to confirm or invalidate that hypothesis. The variation of the isotopic composition of squall lines during their movement from L

I. -.. 1-10107 11-20107 21-31/07 l-lO/OS 11.20108 21-31/08 1-10/09 Time (decade) Kg. 6 Comparison of oxygen-18 contents of rainfalls in periods of 10 days between 1988 and 1989 in Birni N’Konni. in Isotopic study of rainfdl the Sahelian zone (Nigm) 291 east to west has also been studied. In 1989, seven squall lines have been noted. A great depletion of isotopic contents of squall lines during their movement west in June and July can be noted (Fig. 7);in the case of August, it is a lot less noticeable. Figure 8 shows the evolution of deuterium excess from east to west over the four more complete squall lines. At the level of N'Guigmi, the excess of deuterium dis negative, which is the sign of an important evaporation abstracting; then the Zinder d tends to 10, which reveals an oceanic origin of the wet air mass. The evaporation sampling might be less and less important to the west, which is confirmed by a progressive increasing of the relative humidity. Then, between Maradi and Bimi N'Konni, d, which appears to be a lot greater than 10 in the case of mid-season squall lines, could reflect a mixing of oceanic vapour ani of recycled continental vapour coming from water reserves consti- tuted by anterior rainfalls.

Fig. 7 Evolution from east to west of pxygen-18 contents of rainfall. *"

Fig. 8 Evolution from east to west of the excess of deuterium of rainfall. Sf .L

292 J. D. Taupìn mal.

CONCLUSION

The isotopic composition of rainfalls in the tropical zone can bring qualitative elements to the air mass circulation. Due to the complexity of that process, further information must be researched, using other techniques and working on: - the analysis of infrared satellite data in order to separate the altitude of condensa- tion; - climatological maps to define air mass movements; and - radio-samplings to discover the vertical differences between different air layers.

J. J. Acknowledgement The authors are grateful to Prof. Ch. Fontes, Prof. M. Zuppi and A. Filly from Laboratoire d'Hydrologie et de Géochimie Isotopique (Paris XI) for assistance in analysing the samples.

REFERENCES

Joseph, A. & Arranyossy, J. F. (1989) Mise en evidence d'un gradient de contincntaiitt inverse en Afrique de l'Ouest en relation avec les lignes dcgrain. €fydrogeoIogie3,215-218. STUIIY; Mathieu, R., Bariac, T., Fouillac, C., Guillot. B. & Mariotti. A. (1993) Stableisotopevariationsin precipitationsin 1988 and 1989 in Burkina Faso: contributions of regional meteorology. VeiIIe Climanque Sarellíraire 45,4744. il Situatcd northcrr continer been, si graphic In I perforn

c three la collectt tr malySr toire d

RAIN

Accor abund latitut from (Tabe 7 I. from the fc